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黄土高原土壤抗蚀性研究
Alternative TitleA Study on Soil Antierodibility in Loess Plateau
王佑民1; 郭培才2; 高维森3
1994
Source Publication水土保持学报
ISSN1009-2242
Volume8Issue:4Pages:11-16
SubtypeArticle
Contribution Rank3
Abstract土壤抗蚀性是评定土壤抵抗侵蚀能力的重要参数之一,历来为人们所重视。该文根据大量实例资料对黄土高原土壤抗蚀性基本特点进行了分析,认为影响黄土高原土壤抗蚀性的主导因子是腐殖质及粘粒含量;水稳性团粒含量是反映黄土高原土壤抗蚀性的最佳指标;黄土高原土壤抗蚀性可根据土壤腐殖质含量和水稳性团粒含量分为6级;黄土高原土壤抗蚀性的地域分异是东南部最强、西部居中、而北部最弱。
Other AbstractThe antierodibility of soil is one of important indexes for evaluating soil erosion, it is at- ached great importance by soil conservation scentists. This paper explain the main characteristics of soil antierodibility in loess platau based on the data determined, and give main results as fllw. Content of organic matter and clay in sil are dominate facters which impact on soil atierodiblitily inoess plateau. The best index to rllet soil antieroliblity in loesss plateau is content of waterstable ggregaete in soil. Soil atierodibilil in loesss plateau can be divided into six group, acording to con- rent of organic matter and waterstable aggragate. In loess plateau, the soil antierodibility is strong in southwest region, is moderate in west region, and is weakest in north region.
Keyword黄土高原 土壤抗蚀性
DOI10.13870/j.cnki.stbcxb.1994.04.003
Indexed ByCSCD
Language中文
CSCD IDCSCD:247999
Citation statistics
Cited Times:45[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/6377
Collection成都山地所知识仓储(2009年以前)
Corresponding Author王佑民
Affiliation1.西北林学院
2.陕西省黄土高原研究所
3.中国科学院成都山地灾害研究所
Recommended Citation
GB/T 7714
王佑民,郭培才,高维森. 黄土高原土壤抗蚀性研究[J]. 水土保持学报,1994,8(4):11-16.
APA 王佑民,郭培才,&高维森.(1994).黄土高原土壤抗蚀性研究.水土保持学报,8(4),11-16.
MLA 王佑民,et al."黄土高原土壤抗蚀性研究".水土保持学报 8.4(1994):11-16.
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